A multi-element study of ISUA iron-formation, W-Greenland
Meta-sediments from Isua, West Greenland were analyzed by instrumental thermal neutron activation analysis (ITNAA). These sediments are chemical precipitates having some layers of remarkably high Cr content. The latter were compared to Cr poor layers. It turned out that the Cr enriched layers had hi...
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ftnasantrs:oai:casi.ntrs.nasa.gov:19840012893 2023-05-15T16:26:50+02:00 A multi-element study of ISUA iron-formation, W-Greenland Rast, U. Unclassified, Unlimited, Publicly available JAN 1, 1983 application/pdf http://hdl.handle.net/2060/19840012893 unknown Document ID: 19840012893 Accession ID: 84N20961 http://hdl.handle.net/2060/19840012893 No Copyright CASI GEOPHYSICS Lunar and Planetary Inst. Workshop on a Cross Section of Archean Crust; p 71-75 1983 ftnasantrs 2016-06-11T22:53:55Z Meta-sediments from Isua, West Greenland were analyzed by instrumental thermal neutron activation analysis (ITNAA). These sediments are chemical precipitates having some layers of remarkably high Cr content. The latter were compared to Cr poor layers. It turned out that the Cr enriched layers had higher Ir and Ni contents than the samples from the Cr poor layers. Compared to phanerozoic samples the highest Ir contents are not extraordinarily higher than in a modern sediment, and the Cr poor layers, representing more or less phanerozoic shale. From the cratering record of the Moon one can assume a similar cratering of the Earth at about the time when the Isua rocks were formed. Other/Unknown Material Greenland NASA Technical Reports Server (NTRS) Greenland |
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NASA Technical Reports Server (NTRS) |
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ftnasantrs |
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unknown |
topic |
GEOPHYSICS |
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GEOPHYSICS Rast, U. A multi-element study of ISUA iron-formation, W-Greenland |
topic_facet |
GEOPHYSICS |
description |
Meta-sediments from Isua, West Greenland were analyzed by instrumental thermal neutron activation analysis (ITNAA). These sediments are chemical precipitates having some layers of remarkably high Cr content. The latter were compared to Cr poor layers. It turned out that the Cr enriched layers had higher Ir and Ni contents than the samples from the Cr poor layers. Compared to phanerozoic samples the highest Ir contents are not extraordinarily higher than in a modern sediment, and the Cr poor layers, representing more or less phanerozoic shale. From the cratering record of the Moon one can assume a similar cratering of the Earth at about the time when the Isua rocks were formed. |
format |
Other/Unknown Material |
author |
Rast, U. |
author_facet |
Rast, U. |
author_sort |
Rast, U. |
title |
A multi-element study of ISUA iron-formation, W-Greenland |
title_short |
A multi-element study of ISUA iron-formation, W-Greenland |
title_full |
A multi-element study of ISUA iron-formation, W-Greenland |
title_fullStr |
A multi-element study of ISUA iron-formation, W-Greenland |
title_full_unstemmed |
A multi-element study of ISUA iron-formation, W-Greenland |
title_sort |
multi-element study of isua iron-formation, w-greenland |
publishDate |
1983 |
url |
http://hdl.handle.net/2060/19840012893 |
op_coverage |
Unclassified, Unlimited, Publicly available |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland |
genre_facet |
Greenland |
op_source |
CASI |
op_relation |
Document ID: 19840012893 Accession ID: 84N20961 http://hdl.handle.net/2060/19840012893 |
op_rights |
No Copyright |
_version_ |
1766015829890039808 |